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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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GMD | Articles | Volume 13, issue 7
Geosci. Model Dev., 13, 3347–3371, 2020
https://doi.org/10.5194/gmd-13-3347-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Nucleus for European Modelling of the Ocean - NEMO

Geosci. Model Dev., 13, 3347–3371, 2020
https://doi.org/10.5194/gmd-13-3347-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Development and technical paper 30 Jul 2020

Development and technical paper | 30 Jul 2020

Representation of the Denmark Strait overflow in a z-coordinate eddying configuration of the NEMO (v3.6) ocean model: resolution and parameter impacts

Pedro Colombo et al.

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Status: closed
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Pedro Colombo on behalf of the Authors (24 Mar 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Apr 2020) by James R. Maddison
ED: Publish subject to minor revisions (review by editor) (13 May 2020) by James R. Maddison
AR by Pedro Colombo on behalf of the Authors (26 May 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (09 Jun 2020) by James R. Maddison
AR by Pedro Colombo on behalf of the Authors (15 Jun 2020)  Author's response    Manuscript
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Short summary
In the ocean circulation model NEMO, the representation of the overflow of dense Arctic waters through the Denmark Strait is investigated. In this z-coordinate context, sensitivity tests show that the mixing parameterizations preferably act along the model grid slope. Thus, the representation of the overflow is more sensitive to resolution than to parameterization and is best when the numerical grid matches the local topographic slope.
In the ocean circulation model NEMO, the representation of the overflow of dense Arctic waters...
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